마지막 업데이트: 4월 11, 2026
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하이라이트 • 호수
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하이라이트 • 전망대
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하이라이트 • 자연 기념물
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하이라이트 • 해변
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Indeed a very nice fjord on the way to/from the beach. Met a friendly local on the way back to the pier and we had a nice informative chat. Be prepared for a picnic if the café is closed.
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This is a gorgeous little fjord on the way to Bunes beachm often cited as one of Norway's most beautiful beaches. The fjord is hemmed in by Pantaliatinden to the east and Hatinden to the west.
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Stuvdalsvatnet is one of the lakes you'll pass on the way to the Munkebu Hut and the spectacular Munken. You can expect beautiful views along this section. On the trail, there's a rock step that is tackled via a chain – very much necessary when the rock is wet and slippery.
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This is a gorgeous little fjord on the way to Bunes beachm often cited as one of Norway's most beautiful beaches. The fjord is hemmed in by Pantaliatinden to the east and Hatinden to the west.
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This impressive lake is tucked between craggy mountain walls and only separated from the sea by a thin strip. It's used to provide drinking water for the locals and fishing is actively encouraged.
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HISTORY: The area around Meløy has been completely or partially covered by glaciers several times. Around 20,000 years ago, the inland ice was at its greatest extent during the last ice age. In contrast, the glacier was completely ice-free 8,000 and 6,000 years ago. It was only as a result of large amounts of precipitation and a colder climate that the glacier began to grow again 2,500 years ago. In 1750, the glacier tongue was around two kilometers closer to the fjord than it is today. This can be attributed to the visible moraine ridge left by the glacier north and west of Engenbrevatn. The Østertal ice split into two glacier arms around 100 years ago. The eastern one reached as far as the Svartisen glacier lake. Over the next 50 years, the glacier retreated considerably and no longer reached the lake. In 1910 the glacier front was only 50 metres from the glacier lake, but by 1945 it was already 1000 metres away. As the glacier retreated, another glacier lake was formed on the western edge of the glacier arm. As the ice continued to retreat, the lake grew larger from year to year.
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